Active El Niño–Southern Oscillation–like interannual variability 120 million years ago

Abstract The El Niño–Southern Oscillation (ENSO) is the dominant mode of interannual climate fluctuation, generating teleconnections impacting global climate variability today. Its behavior in past greenhouse climates provides a useful perspective for understanding future ENSO under global warming. Despite annually resolved geologic evidence of active ENSO since the Late Cretaceous, ENSO operation at earlier greenhouse periods is poorly resolved. Here, we present evidence from annually resolved lacustrine sediments in northeast China showing signals of interannual precipitation variability 120 m.y. ago, with major frequency bands of 2–5 yr. A coupled climate simulation of the Early Cretaceous generates ENSO-like variability with similar 2–5 yr periodicities in tropical Pacific sea-surface temperatures and atmospheric teleconnection to northeast China precipitation. The Early Cretaceous ENSO-like variability shows higher frequency and stronger amplitude compared to modern ENSO, resembling predictions of future ENSO evolution.

Authors

Institutions

Publication Details

Journal
Geology
Published
2025-09-29
DOI
https://doi.org/10.1130/g53646.1
Citations
1
Primary Topic
Geophysics and Gravity Measurements
Type
article
Field-Weighted Citation Impact
1.79
Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

Active El Niño–Southern Oscillation–like interannual variability 120 million years ago

Yuan Gao, Chengshan Wang, Xing Tian, Jianming Qin et al.
1 citations
Geology
Geophysics and Gravity Measurements
1.79
article

Active El Niño–Southern Oscillation–like interannual variability 120 million years ago

Yuan Gao, Chengshan Wang, Xing Tian, Jianming Qin, Yongyun Hu, Daniel Ibarra, Wenju Cai, Tyler Kukla, Xiang Li, Xiaojing Du, He Huang, Lixin Wu, Jiaqi Guo
article en
1 citations

Abstract

Abstract The El Niño–Southern Oscillation (ENSO) is the dominant mode of interannual climate fluctuation, generating teleconnections impacting global climate variability today. Its behavior in past greenhouse climates provides a useful perspective for understanding future ENSO under global warming. Despite annually resolved geologic evidence of active ENSO since the Late Cretaceous, ENSO operation at earlier greenhouse periods is poorly resolved. Here, we present evidence from annually resolved lacustrine sediments in northeast China showing signals of interannual precipitation variability 120 m.y. ago, with major frequency bands of 2–5 yr. A coupled climate simulation of the Early Cretaceous generates ENSO-like variability with similar 2–5 yr periodicities in tropical Pacific sea-surface temperatures and atmospheric teleconnection to northeast China precipitation. The Early Cretaceous ENSO-like variability shows higher frequency and stronger amplitude compared to modern ENSO, resembling predictions of future ENSO evolution.

GeologyVol. 54(1)
Planetary Science Institute (US), Southwest University (CN), George Mason University (US), Peking University (CN), Brown University (US), NOAA Oceanic and Atmospheric Research (US), China University of Geosciences (Beijing) (CN), Qingdao National Laboratory for Marine Science and Technology (CN), Centre for Southern Hemisphere Oceans Research (AU), Earth and Space Research (US), Ocean University of China (CN)
Openalex Percentile: Top 13%
Geophysics and Gravity Measurements
1.79
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.